AmeriFlux Publications from the Community

Publication Search

Search the Abstract Text

Use the plus button to add multiple search words or phrases.
Author's name
Enter single or multiple author last names for example: franklin, hamilton
Authors: And/Or
- OR
- AND
Site ID(s)
Tip: Use Ctrl-Click (on PC) or Command-Click (on Mac) to select multiple sites.
Select sites
Publication Year From
Publication Year To
Leave blank if not entering a range.

Publications Found: 1437

Response Of Carbon And Water Fluxes To Meteorological And Phenological Variability In Two Eastern North American Forests Of Similar Age But Contrasting Species Composition – A Multiyear Comparison
Beamesderfer, E. R., Arain, M. A., Khomik, M., Brodeur, J. J., Burns, B. M.

The annual carbon and water flux dynamics of two Eastern North American temperate forests were compared over a six-year period from 2012 to 2017. The geographic location, forest age, soil characteristics, and climate were similar between two stands, however, the species composition varied in terms of tree leaf-retention and shape …

Journal: Biogeosciences, Volume 17 (13): 3563-3587 (2020). DOI: 10.5194/bg-17-3563-2020 Sites: CA-TP4, CA-TPD

Atmosphere‐Soil Interactions Govern Ecosystem Flux Sensitivity To Environmental Conditions In Semiarid Woody Ecosystems Over Varying Timescales
Samuels‐Crow, K. E., Ogle, K., Litvak, M. E.

Water and CO2 flux responses (e.g., evapotranspiration [ET] and net ecosystem exchange [NEE]) to environmental conditions can provide insights into how climate change will affect the terrestrial water and carbon budgets, especially in sensitive semiarid ecosystems. Here, we evaluated sensitivity of daily ET and …

Journal: Journal Of Geophysical Research: Biogeosciences, Volume 125 (8): . DOI: 10.1029/2019JG005554 Sites:

Montane Forest Productivity Across A Semiarid Climatic Gradient
Knowles, J. F., Scott, R. L., Biederman, J. A., Blanken, P. D., Burns, S. P., Dore, S., Kolb, T. E., Litvak, M. E., Barron‐Gafford, G. A.

High-elevation montane forests are disproportionately important to carbon sequestration
in semiarid climates where low elevations are dry and characterized by low
carbon density ecosystems. However, these ecosystems are increasingly threatened
by climate change with seasonal implications for photosynthesis and forest growth.
As …

Journal: Global Change Biology, Volume 26 (12): 6945-6958 (2020). DOI: 10.1111/gcb.15335 Sites: US-Fuf, US-MtB, US-NR1, US-Vcm, US-Vcp, US-Vcs

Long‐Term Evapotranspiration Rates For Rainfed Corn Versus Perennial Bioenergy Crops In A Mesic Landscape
Abraha, M., Chen, J., Hamilton, S. K., Robertson, G. P.

Journal: Hydrological Processes, Volume 34 (3): 810-822 (2020). DOI: DOI: 10.1002/hyp.13630 Sites: US-KL1, US-KL2, US-KL3, US-KM1, US-KM2, US-KM3, US-KM4

Cooling And Moistening Of The Planetary Boundary Layer In Interior Alaska Due To A Postfire Change In Surface Energy Exchange
Ueyama, M., Yamamori, T., Iwata, H., Harazono, Y.

Journal: Journal Of Geophysical Research: Atmospheres, Volume 125 (18): (2020). DOI: 10.1029/2020JD032968 Sites: US-Rpf, US-Uaf

Experimental Harvesting Of Wetland Plants To Evaluate Trade-Offs Between Reducing Methane Emissions And Removing Nutrients Accumulated To The Biomass In Constructed Wetlands
Kasak, K., Valach, A., Rey-Sanchez, C., Kill, K., Shortt, R., Liu, J., Dronova, I., Mander, Ü., Szutu, D., Verfaillie, J., Baldocchi, D.

Constructed wetlands built for water treatment often need biomass harvesting to remove nutrients from the system. Usually harvesting is done during the peak growing season to maximize the amount of nutrients removed from the system. This, however, can create huge methane fluxes that escape from plant tissues to the atmosphere. We …

Journal: Science Of The Total Environment, Volume 715: 136960 (2020). DOI: 10.1016/j.scitotenv.2020.136960 Sites: US-Tw5

An Eddy Covariance Mesonet For Measuring Greenhouse Gas Fluxes In Coastal South Carolina
Forsythe, J. D., O’Halloran, T. L., Kline, M. A.

Coastal ecosystems are vulnerable to climate change and have been identified as sources of uncertainty in the global carbon budget. Here we introduce a recently established mesonet of eddy covariance towers in South Carolina and describe the sensor arrays and data workflow used to produce three site-years of flux observations in …

Journal: Data, Volume 5 (4): 97 (2020). DOI: 10.3390/data5040097 Sites: US-HB1, US-HB2, US-HB3

Response Of Soil Co2 Efflux To Shelterwood Harvesting In A Mature Temperate Pine Forest
Thorne, R., Khomik, M., Hayman, E., Arain, A.

In forest ecosystems, soil CO2 efflux is an important component of ecosystem respiration (RE), which is generally driven by variability in soil temperature and soil moisture. Tree harvesting in forests can alter the soil variables, and consequently impact soil CO2 efflux. This study investigated the response of total soil CO2 efflux, …

Journal: Forests, Volume 11 (3): 304 (2020). DOI: 10.3390/f11030304 Sites: CA-TP4

Woody Plant Encroachment Has A Larger Impact Than Climate Change On Dryland Water Budgets
Schreiner-McGraw, A. P., Vivoni, E. R., Ajami, H., Sala, O. E., Throop, H. L., Peters, D. P.

Journal: Scientific Reports, Volume 10 (1): (2020). DOI: https://doi.org/10.1038/s41598-020-65094-x Sites: US-Jo2

Climate Sensitivity Of Peatland Methane Emissions Mediated By Seasonal Hydrologic Dynamics
Feng, X., Deventer, M. J., Lonchar, R., Ng, G. H., Sebestyen, S. D., Roman, D. T., Griffis, T. J., Millet, D. B., Kolka, R. K.

Peatlands are among the largest natural sources of atmospheric methane (CH4) worldwide.
Peatland emissions are projected to increase under climate change, as rising temperatures and shifting
precipitation accelerate microbial metabolic pathways favorable for CH4 production. However, how these
changing environmental factors will …

Journal: Geophysical Research Letters, Volume 47 (17): (2020). DOI: https://doi.org/10.1029/2020GL088875 Sites: US-MBP

Publications

Publication Search

Site Search & Maps

Useful links

01-All
02-None
03-Other
AR-Bal
AR-CCa
AR-CCg
AR-Cel
AR-Rom
AR-TF1
AR-TF2
BR-BNT
BR-Cax
BR-CMT
BR-CST
BR-Cui
BR-CUP
BR-IAB
BR-ITA
BR-Ji1
BR-Ji3
BR-Ma2
BR-Ma3
BR-Moj
BR-Npw
BR-PRS
BR-Sa1
BR-Sa3
BR-SGC
BR-SM1
BR-SM2
BR-SM3
BR-SP1
BR-Xpw
CA-AF1
CA-ARB
CA-ARF
CA-BCW
CA-BOU
CA-BSM
CA-Ca1
CA-Ca2
CA-Ca3
CA-Cbo
CA-CF1
CA-CF2
CA-CF3
CA-Cha
CA-CQ1
CA-CQ2
CA-CQ3
CA-CRB
CA-DB2
CA-DBB
CA-DL1
CA-DL2
CA-DSM
CA-EM1
CA-EM2
CA-EM3
CA-ER1
CA-ER2
CA-Fen
CA-GL3
CA-GL4
CA-Gro
CA-HPC
CA-IQT
CA-JMW
CA-KLP
CA-KT1
CA-KT2
CA-Let
CA-LP1
CA-LU1
CA-LU2
CA-LuM
CA-MA1
CA-MA2
CA-MA3
CA-Man
CA-Mer
CA-MR3
CA-MR5
CA-Mtk
CA-Na1
CA-Na2
CA-NS1
CA-NS2
CA-NS3
CA-NS4
CA-NS5
CA-NS6
CA-NS7
CA-NS8
CA-Oas
CA-Obs
CA-Ojp
CA-PB1
CA-PB2
CA-Qc2
CA-Qcu
CA-Qfo
CA-RBM
CA-RPn
CA-RPp
CA-RSB
CA-SCB
CA-SCC
CA-SF1
CA-SF2
CA-SF3
CA-SJ1
CA-SJ2
CA-SJ3
CA-SMC
CA-ST1
CA-ST2
CA-TP1
CA-TP2
CA-TP3
CA-TP4
CA-TPA
CA-TPD
CA-TVC
CA-WP1
CA-WP2
CA-WP3
CA-WRF
CL-ACF
CL-FJS
CL-OPP
CL-SDF
CL-SDP
CO-GV1
CO-GV2
CR-Dos
CR-Fsc
CR-Lse
CR-Nmr
CR-SoC
MX-Aog
MX-Asf
MX-BRN
MX-CHB
MX-CHN
MX-CLS
MX-EMg
MX-Iit
MX-ISD
MX-Lpa
MX-Oak
MX-PMm
MX-Ray
MX-Sgt
MX-Tes
MX-VQS
PA-Bar
PA-Bas
PE-AMG
PE-BRE
PE-IGP
PE-PAN
PE-QFR
PE-TNR
PR-xGU
PR-xLA
US-A03
US-A10
US-A12
US-A14
US-A20
US-A30
US-A31
US-A32
US-A33
US-A37
US-A38
US-A39
US-A40
US-A41
US-A74
US-AaG
US-ABa
US-ABb
US-ABc
US-ABd
US-ABe
US-ABf
US-AC2
US-AC3
US-AC5
US-AC6
US-Act
US-ADR
US-AF1
US-Akn
US-ALQ
US-AMS
US-An1
US-An2
US-An3
US-AoL
US-AR1
US-AR2
US-ARb
US-ARc
US-ARM
US-ASH
US-ASL
US-ASM
US-Atq
US-Aud
US-AV1
US-AV2
US-AV3
US-AV4
US-AV5
US-Bar
US-BCM
US-Bd4
US-Bd5
US-Bd6
US-BdA
US-BdC
US-Beo
US-Bes
US-BFS
US-BgC
US-Bi1
US-Bi2
US-Bkg
US-Blk
US-Blo
US-BMM
US-Bn1
US-Bn2
US-Bn3
US-BNF
US-Bo1
US-Bo2
US-Br1
US-Br2
US-Br3
US-BRG
US-BRT
US-Brw
US-Bsg
US-BSM
US-BTL
US-BWa
US-BWb
US-BWe
US-BZB
US-BZF
US-BZL
US-BZo
US-BZS
US-CAK
US-CaV
US-CC1
US-CC2
US-CdM
US-Ced
US-CF1
US-CF2
US-CF3
US-CF4
US-CGG
US-ChR
US-CLF
US-CLN
US-CLS
US-Cms
US-CMW
US-CN1
US-CN2
US-Cop
US-CPF
US-CPk
US-CPR
US-CRE
US-CRK
US-CRT
US-CRW
US-CS1
US-CS2
US-CS3
US-CS4
US-CS5
US-CS6
US-CS7
US-CS8
US-Cst
US-Ctn
US-CU1
US-CU2
US-CU3
US-CU4
US-CwG
US-Cwt
US-CX1
US-CX2
US-CZ1
US-CZ2
US-CZ3
US-CZ4
US-DBk
US-DCS
US-Dea
US-Deu
US-DFC
US-DFK
US-Dia
US-Dix
US-Dk1
US-Dk2
US-Dk3
US-Dmg
US-DPP
US-DPW
US-DS1
US-DS2
US-DS3
US-DUF
US-E32
US-EA4
US-EA5
US-EA6
US-EDN
US-EKH
US-EKN
US-EKP
US-EKY
US-Elm
US-ELW
US-EML
US-EPM
US-Esm
US-EvM
US-FBE
US-Fcr
US-Fmf
US-Fo1
US-Fo2
US-FPe
US-FR1
US-FR2
US-FR3
US-Fuf
US-Fwf
US-GBT
US-GCE
US-GL1
US-GL2
US-GLE
US-GMF
US-Goo
US-GR8
US-GR9
US-GZ1
US-GZ2
US-GZ3
US-Ha1
US-Ha2
US-Ha3
US-HAR
US-HB1
US-HB2
US-HB3
US-HB4
US-HB5
US-HB6
US-HB7
US-HBa
US-HBb
US-HBK
US-Hn1
US-Hn2
US-Hn3
US-Ho1
US-Ho2
US-Ho3
US-HPY
US-HRA
US-HRC
US-HRN
US-HRo
US-HRP
US-HRS
US-Hsm
US-HVa
US-HVs
US-HWB
US-IAA
US-IAB
US-IAC
US-IAM
US-IB1
US-IB2
US-ICh
US-ICs
US-ICt
US-IL1
US-INa
US-INb
US-INc
US-INd
US-INe
US-INf
US-INg
US-INi
US-INj
US-INn
US-INp
US-IS1
US-IS2
US-IS3
US-Ivo
US-JER
US-JFM
US-JFP
US-JLN
US-JLR
US-Jo1
US-Jo2
US-Jo3
US-JRn
US-Jxg
US-Jxn
US-Jxs
US-K4B
US-KCM
US-KEY
US-KFB
US-KFS
US-KGF
US-KL1
US-KL2
US-KL3
US-KLI
US-KLS
US-KM1
US-KM2
US-KM3
US-KM4
US-Knz
US-Kon
US-KPL
US-KS1
US-KS2
US-KS3
US-KS4
US-KSA
US-KSC
US-KSP
US-KUO
US-KUT
US-Kyv
US-LA1
US-LA2
US-LA3
US-LBJ
US-LCW
US-LGr
US-Lin
US-LL1
US-LL2
US-LL3
US-LMA
US-LMB
US-LMS
US-LMW
US-Los
US-LPH
US-LS1
US-LS2
US-LU1
US-LWW
US-MAC
US-MBP
US-MC1
US-MC2
US-MCP
US-Me1
US-Me2
US-Me3
US-Me4
US-Me5
US-Me6
US-Me7
US-MEF
US-Men
US-MFs
US-MG1
US-MH1
US-MH2
US-Mi1
US-Mi2
US-Mi3
US-Mj1
US-Mj2
US-MKG
US-MKH
US-MKN
US-MMS
US-MN1
US-MN2
US-MN3
US-Mo1
US-Mo2
US-Mo3
US-MOz
US-Mpj
US-MRf
US-MRM
US-MSR
US-MtB
US-Mur
US-MVF
US-MVW
US-MWA
US-MWF
US-MWo
US-MWS
US-MWU
US-MWW
US-Myb
US-MZA
US-NC1
US-NC2
US-NC3
US-NC4
US-NC5
US-Ne1
US-Ne2
US-Ne3
US-NGB
US-NGC
US-NMj
US-NOG
US-NP1
US-NP2
US-NR1
US-NR2
US-NR3
US-NR4
US-Nrf
US-Nrs
US-NSa
US-NSb
US-NSW
US-NWT
US-NYa
US-NYb
US-NYc
US-NYd
US-NYe
US-NYf
US-NYg
US-NYh
US-NYi
US-NYj
US-NYk
US-NYl
US-NYm
US-NYn
US-NYo
US-NYp
US-NYq
US-NYr
US-OF1
US-OF2
US-Oho
US-OK1
US-OK2
US-ONA
US-OPE
US-ORv
US-OSB
US-OWC
US-PAS
US-PeA
US-PFa
US-PFb
US-PFc
US-PFd
US-PFe
US-PFf
US-PFg
US-PFh
US-PFi
US-PFj
US-PFk
US-PFL
US-PFm
US-PFn
US-PFo
US-PFp
US-PFq
US-PFr
US-PFs
US-PFt
US-PHM
US-PiU
US-PLM
US-PLo
US-Pnp
US-Pon
US-Prr
US-PSH
US-PSL
US-PVA
US-Px1
US-Px2
US-Px3
US-Px4
US-Px5
US-RC1
US-RC2
US-RC3
US-RC4
US-RC5
US-RFE
US-RFW
US-RGA
US-RGB
US-RGF
US-RGG
US-RGo
US-RGR
US-RGW
US-Rls
US-Rms
US-Ro1
US-Ro2
US-Ro3
US-Ro4
US-Ro5
US-Ro6
US-Rpf
US-RRC
US-RTS
US-Rwe
US-Rwf
US-Rws
US-Sag
US-SB1
US-SB2
US-SB3
US-SBC
US-SBR
US-SCc
US-SCd
US-SCf
US-SCg
US-SCm
US-SCs
US-SCw
US-SD1
US-SD2
US-SdH
US-SDU
US-Seg
US-SER
US-Ses
US-SFP
US-SHC
US-Shd
US-SHS
US-Si1
US-Si2
US-SJ1
US-SJ2
US-Skr
US-Slt
US-SM1
US-Snd
US-Sne
US-Snf
US-SO2
US-SO3
US-SO4
US-SP1
US-SP2
US-SP3
US-SP4
US-SRC
US-SRE
US-SRG
US-SRM
US-Srr
US-SRS
US-SSH
US-Sta
US-StJ
US-StS
US-SuM
US-SuS
US-SuW
US-SVC
US-SVP
US-Sx1
US-Sx2
US-Sx3
US-Syv
US-SZ1
US-SZ2
US-SZ3
US-TaS
US-TCS
US-TEF
US-TFF
US-TKs
US-TLR
US-Ton
US-TrB
US-TrS
US-Tsm
US-Tur
US-Tw1
US-Tw2
US-Tw3
US-Tw4
US-Tw5
US-Twt
US-Tx1
US-Tx2
US-Tx3
US-Tx4
US-Tx5
US-Tx6
US-Tx7
US-Tx8
US-Tx9
US-Uaf
US-UC1
US-UC2
US-UG1
US-UiA
US-UiB
US-UiC
US-UiD
US-UiE
US-UiF
US-UiG
US-ULM
US-UM3
US-UMB
US-UMd
US-UND
US-Upa
US-UR0
US-UR1
US-UR2
US-UR3
US-UR4
US-UR5
US-UR6
US-UR7
US-UR8
US-UR9
US-UTB
US-UTD
US-UTE
US-UTG
US-UTJ
US-UTL
US-UTM
US-UTN
US-UTP
US-UTV
US-UTW
US-UUC
US-UUP
US-Var
US-Vcm
US-Vcp
US-Vcs
US-VFP
US-VT1
US-VT2
US-WBW
US-WCr
US-Wdn
US-WEP
US-Wgr
US-Whs
US-Wi0
US-Wi1
US-Wi2
US-Wi3
US-Wi4
US-Wi5
US-Wi6
US-Wi7
US-Wi8
US-Wi9
US-Wjs
US-Wkg
US-Wlr
US-WOD
US-Woo
US-Wpp
US-WPT
US-Wrc
US-WT1
US-WT2
US-WT3
US-Wwt
US-xAB
US-xAE
US-xBA
US-xBL
US-xBN
US-xBR
US-xCL
US-xCP
US-xDC
US-xDJ
US-xDL
US-xDS
US-xGR
US-xHA
US-xHE
US-xJE
US-xJR
US-xKA
US-xKZ
US-xLE
US-xMB
US-xML
US-xNG
US-xNQ
US-xNW
US-xPU
US-xRM
US-xRN
US-xSB
US-xSC
US-xSE
US-xSJ
US-xSL
US-xSP
US-xSR
US-xST
US-xTA
US-xTE
US-xTL
US-xTR
US-xUK
US-xUN
US-xWD
US-xWR
US-xYE
US-YK1
US-YK2
US-Ylw
US-YNS
US-ZF1
US-ZF2

Publication Search

Page 14 of 144 pages

First Page | Last Page | Middle Page

Site Search & Maps

Useful links

First Page |

Last Page |

Middle Page